ad th la record from Greenland Ice Core GISP2 show a close correlation of sea-surface water conditions and deep-sea contouritic sedimentation in the Gulf of Cadiz with Northern Hemisphere climate variability on millennial timescales. A high MOW velocity Dansgaard-Oeschger (D-O) stadials and intersta...
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.9091 http://www.epoc.u-bordeaux.fr/indiv/Zaragosi/Toucanne_et_al_2007a.pdf |
Summary: | ad th la record from Greenland Ice Core GISP2 show a close correlation of sea-surface water conditions and deep-sea contouritic sedimentation in the Gulf of Cadiz with Northern Hemisphere climate variability on millennial timescales. A high MOW velocity Dansgaard-Oeschger (D-O) stadials and interstadials been recognized as far south as the Portuguese margin |
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